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Inventory of Plants, Plant 

Communities and Herpetofauna of 

Concem in the \^cinity of the 

Snow-Talon Bum, Helena 

National Forest 



Prepared for: 

Helena National Forest 

2880 Skyway Drive 
Helena, Montana 59602 



By: 

Stephen V. Cooper, Gregory M. Kudray, Paul Hendricks, Bryce A. Maxell, 
W. Marc Jones, Cobum Currier and Susan Lenard 



Montana Natural Heritage Program 

Natural Resource Information System 

Montana State Library 



December 2005 




MONTANA 



^ Natural Heritage 
Pix^^ram 



Inventory of Plants, Plant 

Communities and Herpetofauna of 

Concem in the \^cinity of the 

Snow-Talon Bum, Helena 

National Forest 



Prepared for: 

Helena National Forest 

2880 Skyway Drive 
Helena, Montana 59602 



Agreement Number: 
03-CS-11011200-007 

By: 

Stephen V. Cooper, Gregory M. Kudray, Paul Hendricks, Bryce A. Maxell, 
W. Marc Jones, Cobum Currier, and Susan Lenard 



j^T" MONTANA 

'l^ Natural Heritage 




^t ^-^ MUSTAFA j'j/'dAA Un-NTAllA 

^T^itate If jIV Natuial Kesounx 

^ Library ^^jjjP MMmation System 



© 2005 Montana Natural Heritage Program 
P.O. Box 201800 • 1515 East Sixth Avenue • Helena, MT 59620-1800 • 406-444-5354 



This document should be cited as follows: 

Cooper, S.V., G. M. Kudray, P. Hendricks, B.A. Maxell, Jones, W. M., C. Currier, and S. Lenard 2005. 
Inventory of Plants, Plant Communities, and Herpetofauna of Concern in the Vicinity of the Snow-Talon 
Burn, Helena National Forest. Report to the Helena National Forest. Montana Natural Heritage 
Program, Helena, MT. 15 pp. plus appendices. 



Executive Summary 



Montana Natural Heritage Program (MTNHP) 
biologists inventoried sensitive vascular plants, 
riparian and wetland associated plant communities, 
and herpetofauna near and within the Snow-Talon 
Fire of 2003 on the Helena National Forest. 
Appropriate habitat was searched for 14 vascular 
plant species of concern that are potentially present 
in the area, however, none were encountered. 
Ninety percent of the twenty sites had 
herpetofauna with four amphibian species (Long- 
toed Salamander, Rocky Mountain Tailed Frog, 
Western Toad, and Columbia Spotted Frog) and 
two reptile species (Terrestrial Gartersnake and 
Common Gartersnake) recorded. Detections of 
the Western Toad, a Montana Species of Concern 
as well as a U.S. Forest Service Northern Region 
Sensitive Species (MTNHP 2004), were 
noteworthy and encouraging. It was breeding in all 
four drainages surveyed, indicating that a relatively 
large population is now in the area and is possibly 
expanding because of the fire and the Western 
Toad preference for disturbed forest and wetland 
habitats. This is especially significant given 
declining trends for this species elsewhere in 
western Montana during the last 50 years. We 
recommend monitoring of Western Toad 
populations in the area and systematic surveys of 
stream habitats in order to better document the 
distribution and status of Rocky Mountain Tailed 
Frogs in the area; there is only one record in this 
locale other than the two sites we found. 

Detailed vegetation surveys were conducted at 
several wetland and riparian sites. Baseline early 
post-burn vegetation data will enable further 
monitoring of the effects of wildfire on vegetation 
and herpetofauna habitat in these important 
ecosystems. About half of the 50 potentially 
occurring riparian and wetland plant communities 
having a rank of G3, S3, or less were documented. 



Generally, these sites were ecologically intact and 
represented important habitat in this relatively arid 
environment. A few sites are unique and the 
diversity of wetland plant communities is 
considerable. 

One large wetland (Copper Creek, Lower 
Drainage site) contained an extensive carr, a type 
of fen, which is a very uncommon community type 
in Montana. This site has an extensive bryophyte 
component and warrants further survey for this 
taxonomic group. At Porcupine Basin we 
putatively identified the easternmost documentation 
of Northern licorice-root, a species more typically 
found in mesic northern Idaho. The lack of seeds 
for a positive identification suggests that another 
visit at the appropriate time would be worthwhile, 
as this would be a considerable range extension. 

Keep Cool Lakes has a community type that may 
have once been a species-rich blue wildrye 
meadow, a G2 rank community previously known 
only from California and Oregon. Nonnative 
timothy grass now dominates. Keep Cool Lakes is 
still an intact and diverse wetland, but typifies a 
problem often encountered when ATV use occurs 
in these open and easily accessible types. 
Nonnative species were invading along the 
disturbed track, one vegetation type was degraded, 
and large disturbances were created where ATVs 
had to be extricated from wetter areas. Western 
toads were breeding here and ATV tracks were 
noted within a few feet of where toads were 
depositing egg strings. 

The ecological integrity of this site and most other 
accessible wetlands will be threatened if the 
disturbance and resultant weed infestation and 
habitat degradation from ATV use continue. 



N 



Acknowledgments 

The work described in this report was funded status of wetland habitats and wetland dependent 
primarily through Challenge Cost Share Agreement species on the Helena National Forest. We would 

No. 03-CS-11011200-007 between the Helena also like to acknowledge the Region 1 Office of the 

National Forest and the Nature Conservancy's US Forest Service for their continued support of 

Montana Natural Heritage Program. We are the statewide amphibian inventory program; data 

particularly grateful to Lois Olsen of the Helena from this project is included in the report. 
National Forest for her interest in evaluating the 



VI 



Table of Contents 

Introduction 

Methods 

Botanical and Community Surveys 

Herpetofauna Surveys 

Data Management 

Results and Discussion 3 

Herpetofauna 3 

Sensitive Plants and Communities 5 

Conclusions / Recommendations 13 

Herpetofauna 13 

Sensitive Plants and Communities 13 

Literature Cited 14 

List of Figures 

Figure 1 . Study area and ecological survey areas in the vicinity of the Snow-Talon burn 2 

Figure 2. Wetlands surveyed for herpetofauna in 2004 and 2005 4 

Figure 3. ATV track through Keep Cool Lake wetlands 9 

Figure4. Drawdown zone at Reservoir Lake 11 

Figures. Porcupine Basin wet meadow 12 



Appendix A. Global/State Rank Definitions 
Appendix B . Tables 

Table 1 . Inventory targets for plant species of concern and highly ranked plant 

communities Appendix B - 1 

Table 2. Amphibian and reptile species detected during wetland site surveys Appendix B - 2 

Appendix C. Occurrence Maps of Herpetofauna 

Figure 1. Long-toed Salamander {Amby stoma macrodactylum) Appendix C - 1 

Figure 2. Rocky Mountain Tailed Frog (Ascaphus montanus) Appendix C - 2 

Figure 3. Western Toad (Bufo boreas) Appendix C - 3 

Figure 4. Columbia Spotted Frog {Rana luteiventris) Appendix C - 4 

Figures. Terrestrial Gartersnake (Thamnophis elegans) Appendix C - 5 

Figure 6. Common Gartersnake {Thamnophis sirtalis) Appendix C - 6 



vn 



Introduction 

The summer of 2003 was an extreme fire year 
throughout the western US and western Montana, 
where one extensive fire, the Snow-Talon, 
occurred on the Helena National Forest near 
Lincoln (Figure 1). The USFS contracted with the 
Montana Natural Heritage Program to conduct a 
survey to gauge the impact of the fire on some of 
the wetland systems and a selected portion of their 
biota. Another objective was to understand the 
diversity of wetlands within a core area that 
included the burned area as well as some outlying 
sites. This survey can serve as a baseline to help 
predict fire effects on herpetofauna in similar 
ecosystems and to evaluate post fire succession. 

Methods 

We conducted surveys in the late spring and 
summer of 2004 and 2005 that were focused on 
plant and amphibian species of concern (Appendix 
B Tables 1 and 2) and priority vegetation types 
(plant associations) associated with wetland/ 
riparian habitats. Lois Olsen, Ecologist for the 
Helena National Forest, made informed suggestions 
as to which drainages and wetlands were of 
highest potential interest. 

Botanical & Community Surveys 

We compiled a list (Appendix B Table 1) of highly 
ranked communities, those with a Global (G) or 
State (S) rank of 3 or less or where S-rank was 
currently undetermined (Grossman et al. 1998, 
Anderson et al. 1998). Forest Service Sensitive 
plant species (Appendix B Table 1) likely to occur 
in the study area were also identified. Further 
information on these plants and communities can be 
obtained from the Montana Natural Heritage 
Program's web site, www.mtnhp.org and "Plant 
Species of Concern" by the Montana Natural 
Heritage Program (2003). In the field, we sampled 
vegetation communities by structure and 
composition with emphasis on dominants and 
indicator species. Vegetation keys and descriptions 
(Pfister et al. 1977, Hansen et al. 1995) were 
consulted to verify vegetation associations at sites. 
Some communities did not key to or match 
descriptions in either of the above references. 



When this was the case, we then consulted the 
EcoART database (ABI 2000) and attempted to 
match communities to those in the database. 

Herpetofauna Surveys 

Sites for amphibian surveys were identified through 
discussions with the Heritage Program wetland 
ecologist, Helena National Forest personnel, and 
study of USGS 7.5' topographic maps. Marshes, 
small ponds and lakes, and selected stream reaches 
in the study area, all of which were north of 
Lincoln on Helena National Forest lands in Lewis 
and Clark and Powell counties, were priority sites 
for surveys. 

Shorelines and wetland margins were searched for 
adults and juveniles while walking along the edge. 
The entire perimeter was searched at some sites, 
others were inspected by traversing the length of 
the site through shallow emergent vegetation, or 
along selected portions of the margin where 
emergent vegetation or other cover was present. 
June surveys included visual searches for egg 
masses attached to submerged and emergent 
vegetation or egg strings in shallow open water. At 
regular intervals, and where appropriate, the 
aquatic habitat was sampled for larvae using a 
dipnet. 

Time of day and duration of searches (a measure 
of search effort: Heyer et al. 1994, Olson et al. 
1997), weather, water temperature, and species 
encountered were recorded on standard U.S. Fish 
and Wildlife Service data sheets. Duration of site 
surveys ranged from 9-300 minutes (Appendix B 
Table 2), and depended upon the size and structural 
complexity of each site, site conditions (including 
weather), and findings. A team of two or three 
persons conducted each survey. 

Data Management 

New data collected on amphibians, plant species of 
concern, and high quality vegetation communities 
were georeferenced, digitized and documented as 
element occurrence records in the databases 
maintained by the Montana Natural Heritage 
Program. Plot data and summary information on 
noteworthy sites were also entered into MTNHP 



1 



^ ^^^ V^ O X T A N A 

/ Ji\ Natural 




Figure 1. Study area and ecological survey areas near the Snow-Talon burn 



databases. This data system serves as the primary 
source of information on the status and distribution 
of Montana's native species and habitats. 

Results and Discussion 
Herpetofauna 

In 2004 we conducted 20 site surveys for 
amphibians (Figure 2, Appendix B Table 2) in the 
drainages of Beaver Creek (sites 11, 19-20), 
Copper Creek (sites 8-10, 14-18), Keep Cool 
Creek (sites 1-2), and Landers Fork (sites 3-7, 12- 
13). Sites ranged in elevation from 4900 ft to 7220 
ft and were surveyed during 1-4 June or 8-9 
September; all sites were visited only once. In 
2005, 7 of these sites were resurveyed and an 
oxbow on the Blackfoot River (site 21) was also 
surveyed because of previous records of Western 
Toad breeding activity at these locations (Figure 2 
& Appendix C Figure 5, Appendix B Table 2). 
Four amphibian species (Long-toed Salamander, 
Rocky Mountain Tailed Frog, Western Toad, 
Columbia Spotted Frog) and two reptile species 
(Terrestrial Gartersnake and Common 
Gartersnake) were detected during the surveys. 
No amphibians or reptiles were found at two (10%) 
of the sites we surveyed. The most commonly 
observed amphibian during our 2004 surveys was 
the Columbia Spotted Frog, detected at 13 sites. 
The Rocky Mountain Tailed Frog was found at two 
sites, the Long-toed Salamander at one site, the 
Terrestrial Gartersnake at one site, and the 
Common Garter Snake at one site. The Western 
Toad was detected at nine sites in 2004 and 
detected breeding at 5 of the 8 sites resurveyed in 
2005 when they were the focus of survey effort. 

We found evidence of breeding in the study area by 
four of the amphibian species detected in both 2004 
and 2005: Long-toed Salamander at one site (5%) 
in 2004 and five sites (63%) in 2005, Rocky 
Mountain Tailed Frog at the only two sites (100%) 
surveyed in 2004 which had suitable habitat 
present. Western Toad at five sites (25%) in 2004 
and five sites (63%) in 2005, and Columbia Spotted 
Frog at ten sites (50%) in 2004 and three sites 
(38%) in 2005 (Appendix B Table 2, Figure 2, 
Appendix C Figures 1-6). Long-toed Salamanders, 



Western Toads, and Columbia Spotted Frogs were 
documented breeding in each of the four drainages 
we sampled as well as at the oxbow on the 
Blackfoot River. Rocky Mountain Tailed Frogs 
were detected only in the Beaver Creek drainage. 
However, this was the only drainage where suitable 
stream habitats were surveyed. As indicated by 
the presence of another observation of the species 
on a tributary to Copper Creek in 1966, it seems 
likely that additional surveys of suitable stream 
habitats would reveal their presence throughout 
much of the area. 

During the 2004 surveys, we found all native 
amphibian species expected in the study area. 
Three additional native amphibian species found in 
Montana west of the Continental Divide, Coeur 
d'Alene Salamander (Plethodon idahoensis), 
Pacific Treefrog (Pseudacris regilla) and 
Northern Leopard Frog {Rana pipiens), have not 
yet been reported from either Powell or Lewis and 
Clark counties (Maxell et al. 2003, Werner et al. 
2004). 

Of the four amphibian species present, the Western 
Toad is a Montana Species of Concern, as well as 
a U.S. Forest Service Northern Region Sensitive 
species (Montana Natural Heritage Program 
2004). It is noteworthy that we not only detected 
them in all four drainages that we surveyed, but 
that we detected them breeding at 25% of the sites 
surveyed in 2004. This is especially encouraging 
given apparent declining trends for this species 
elsewhere in western Montana during that last 50 
years and region wide detection of breeding at only 
2-5% of sites surveyed in recent years (Maxell 
2000, 2004; Maxell et al. 2003; Werner et al. 2004). 

Factors affecting breeding toads in western 
Montana and the sites they use for breeding are not 
entirely clear. However, there is growing evidence 
from surveys conducted by the statewide 
amphibian inventory program, as well as research 
being conducted in Glacier National Park, that 
stand replacing fires are beneficial to Western 
Toads. These fires open up both aquatic and 
terrestrial habitats to greater solar exposure and 
may also provide more terrestrial burrows by 
loosening soils and burning out tree roots (Maxell, 




Site numbers correspond 
to those in Table 2 



N 

S 



0.9 1.8 Miles 
_J I 




M O !Si T A N A 

Natiaral 
Heritage 
Program 



Figure 2. Wetlands surveyed for herpetofauna in 2004 and 2005 

4 



personal observation; Steve Corn and Blake 
Hossack, Aldo Leopold Wilderness Research 
Institute, personal communication). Our detections 
and observations corroborate these findings. We 
found adult Western Toads in several wetlands 
within the Copper Creek drainage and Indian 
Meadows that experienced extensive fire 
disturbance in 2003. The season when fires occur 
may be important. Adult Western Toads breed 
earlier in the year than the typical peak of fire 
season and are able to seek refuge during autumn 
fires. Late summer and autumn fires could impact 
tadpoles and recent metamorphs. However, toads 
can live 20 years or more once they reach 
adulthood, a life span that could include many years 
of complete reproductive failure. 

One factor known to affect successful breeding is 
trampling or similar disturbance. At Upper Keep 
Cool Lake (site 1 in Figure 2 and Appendix B Table 
2) we found recent ATV tracks in the wet meadow 
as well as within the water within a few feet of 
where toads were depositing egg strings in 2004 
and observed similar evidence of ATV use on our 
visit in 2005 when the site was virtually dry. 
Motorized activity in wet meadows could severely 
affect toad breeding. At known toad breeding sites 
where the public tends to concentrate, signs could 
be posted to remind the public that such activity is 
banned for that specific reason, as well as to 
protect vulnerable wet meadow and near- shore 
wetland habitats. 

Sensitive Plants & Communities 

The information below is summarized from notes 
taken during surveys of late August 2004 and 
organized by site (Figure 1) in alphabetical order. 

• Copper Creek, Upper Drainage: Two 

pond-centered wetlands were inventoried near 
the headwaters of Copper Creek. These 
depressional wetlands probably resulted from 
glacial scouring of Belt Series bedrock 
(primarily argillite) leaving relatively shallow 
excavations with a somewhat impermeable 
substrate into which headwaters drain and pond 
before overflowing. The more southerly of the 
two ponds has dried significantly (no standing 
water) from what is portrayed on the Stonewall 



Mountain USGS 1 :24,000 quadrangle map; the 
previous six droughty years may have resulted 
in the mudflat condition that now exists. The 
lowest portion of the (former) pond is a mudflat 
dominated by a tussock form of water sedge 
(Carex aquatilis); tufted hairgrass 
(Deschampsia cespitosa) is scattered as well. 
The most conspicuous forb is a species of 
pussytoes (Antennaria). Exposed gravel and 
rock, once underwater, forms a concentric zone 
about the mudflat. The Snow-Talon Fire 
burned up to the perimeter of the pond but 
there was no obvious evidence that the wetland 
vegetation had burned. 

The considerably larger, more northerly pond 
has not suffered any perceptible drawdown and 
is completely encircled by wetland vegetation. 
The Snow-Talon Fire burned through all the 
different vegetation types surrounding the pond 
with variable effects but was most noticeable in 
the forested portion of the wetland. 

Engelmann spruce - subalpine fir / Claspleaf 
twistedstalk (Picea engelmannii - Abies 
lasiocarpa / Streptopus amplexifolius) and 
Engelmann spruce / field horsetail {P. 
engelmannii / Equisetum arvense) are the 
two major plant associations comprising the 
forested portion of the wetland (less than Va of 
the ponds perimeter) where water input from 
upslope feeder streams was concentrated. 
This highly oxygenated water may explain the 
presence of trees here and not in other 
perimeter areas where water is stagnant and 
oxygen depleted. More than half of the trees, 
predominantly Engelmann spruce, but including 
subalpine fir and lodgepole pine {Pinus 
contorta) were killed by the fire. The 
undergrowth experienced fire of varying 
intensities but has responded with vigor, 
probably due to a post-burn fertilization effect. 
The undergrowth dominants are arrowleaf 
ragwort (Senecio triangularis), Canby's 
licorice-root (Ligusticum canbyi), Trollius 
laxus (American globeflower), green false 
hellebore (Veratrum viride), claspleaf 
twistedstalk, Parnassia fimbriata (fringed 
grass-of-Parnassus), broadleaf arnica (Arnica 



latifolia), and blue wildrye (Elymus glaucus). 
Grouse whortleberry (Vaccinium scoparium) 
and rusty menziesia {Menziesia ferruginea) 
were scattered on higher ground, often 
encircling tree bases. A stream through the 
forested wetland supports a liverwort species 
on completely submerged stream gravels. The 
streambank was colonized in large part by 
Sphagnum squarrosum (and/or S. teres). 

The perimeter of the area post fire now is 
dominated by herbaceous species; however 
about two thirds of the perimeter appears to 
have previously been shrub/dwarf- shrub- 
dominated. All shrub species are resprouting, 
but given only a partial season of post-fire 
growth, their heights are uniformly less than 2 
dm. Prior to the fire about a third of the pond's 
perimeter was occupied by herbaceous 
communities dominated by beaked sedge 
(Carex utriculata) or bluejoint reedgrass 
{Calamagrostis Canadensis). Shrub 
communities are dominated by willow (Salix) 
species, primarily Booth' willow (S. boothii) 
and to a lesser extent, Tweedy's willow (5. 
tweedyi) which is confined to beaver (Castor 
canadensis) workings. Bog laurel (Kalmia 
polifolia) and rose meadowsweet (= rose 
spiraea. Spiraea splendens) are minor 
components. The undergrowth of these 
shrublands is primarily dominated by beaked 
sedge and/or water sedge and to a lesser 
degree bluejoint reedgrass. The shrub 
communities are on raised areas created by 
former beaver use. The beaked sedge 
community ranged from near total dominance 
by this species to equal mixes of beaked sedge 
and water sedge and/or bluejoint reedgrass / 
northern reedgrass (C striata). Timber 
oatgrass (Danthonia intermedia), a species 
typically associated with dry sites, quite 
unexpectedly was scattered in some saturated 
areas here. Primary forb species included 
scentbottle (Platanthera dilatata = 
Habenaria dilatata), Rocky Mountain 
groundsel (Packera streptanthifolia = 
Senecio streptanthifolius), twinleaf bedstraw 
(Galium bifolium), sticky tofieldia (Tofieldia 
glutinosa) and elephanthead lousewort 



(Pedicularis groenlandica). The primary 
willow species are Booth's willow and 
Tweedy's willow; these two species are 
dominant on old beaver workings, beaked 
sedge is the dominant herb. A variety of 
bryophytes, including Aulacomnium palustre, 
Bryum pseudotriquetrum, Bryum spp., 
Polytrichum spp. and especially Sphagnum 
spp. form a rather continuous ground layer. 

Fragments of several different community 
types (1-5 m along their longest axis) were 
developed on what appeared to be peat 
deposits (the depth of peat was not measured, 
but it is likely that the histic epipedon was of 
insufficient depth to qualify these sites as 
peatlands). Sedge tussocks (Carex spp., 
unidentified due to immature inflorescence) 
constituted 40-70% canopy cover. They were 
dispersed over a substrate that was mostly very 
shallow standing water with a submerged lawn 
of mosses. Scorpidium spp. is dominant with 
Bryum pseudotriquetrum and Aulacomnium 
palustre common. The provisionally 
recognized Tweedy's willow / bluejoint 
reedgrass shrubland, a plant community not 
described at either the state or national level, 
occurs in small patches on substrates with 
better drainage than those supporting other 
willow communities in this complex. This 
Tweedy's willow-dominated community 
occupies essentially the same habitat as the 
Geyer's willow (Salix geyeriana)/ bluejoint 
reedgrass shrubland in which Booth's willow is 
considered an ecological analogue of Geyer's 
willow for purposes of management oriented 
classification (Hansen et al. 1995). For 
tracking diversity it is probably prudent to 
recognize the Tweedy's willow / bluejoint 
reedgrass community as unique; it can be 
lumped with Geyer's willow type for mapping 
and management purposes. 

No sensitive plants were found within 
these wetlands or in the near vicinity. 

» Copper Creek / North Fork Creek 
Confluence: This wetland complex was near 
the confluence of Copper Creek with North 



Fork Creek. Just west of the confluence of 
these creeks is a forested and shrub-dominated 
wetland that burned at various intensities. The 
forested plant associations Engelmann spruce / 
field horsetail and Engelmann spruce / bluejoint 
reedgrass occur in a complex mosaic with the 
last named occupying sites lower in the 
landscape (wetter) and the former occurring in 
slightly higher positions (by 1-4 dm). In 
addition to Engelmann spruce, lodgepole pine 
dominates (or at one time dominated) the 
overstory and mature subalpine fir is scattered 
within the drier association. Bluejoint 
reedgrass forms a particularly lush cover, 
hypothetically due to a post-bum fertilization 
effect and the reduced tree canopy; 
incorporated in this tall grass layer is fringed 
brome (Bromus ciliatus) and two alien species, 
redtop {Agrostis gigantea = A. alba) and 
quackgrass (Elymus repens = Agropyron 
repens). Forbs, including Lyall's angelica 
{Angelica arguta), giant mountain aster 
(Canadanthus modestus = Aster modestus), 
and alpine leafybract aster (Symphyotrichum 
foliaceum = A. foliaceus), are a modest 
component of this type with a combined cover 
of less than 10 % throughout most of the 
mosaic. Robust populations of the noxious 
weed Canada thistle (Cirsium arvense) are 
also present; whether this incursion occurred 
prior to the fire or following is unknown. 
Inclusions of diamondleaf willow {Salix 
planifolia) / beaked sedge are present with the 
willow reduced to root-crown sprouting 
following the fire. 

A tall willow community existed prior to the fire 
closer to the confluence. The fire burned over 
the willows killing them back to the base but 
virtually all clumps are vigorously root-crown 
sprouting. The primary plant associations 
present are Geyer's willow / beaked sedge, 
Booth's willow / beaked sedge. Booth's willow 
/ bluejoint reedgrass, and diamondleaf willow / 
beaked sedge. The mix of these vigorously 
sprouting clumps of the two willows is so 
complex on a fine scale that distinguishing 
individual community types is quite pointless 
(situations like this prompted Hansen et al. 



[1995] to declare ecological equivalence of the 
two willow species, using Geyer's willow as 
the nominal). The grasses and sedges in the 
willow complex are also quite lush, forming 
nearly complete coverage, a condition that can 
be contrasted with the pre-burn situation where 
the graminoid and forb components are usually 
quite inconspicuously mixed between clumps of 
10-20 ft tall willows. If one were to categorize 
the current status of the former willow swamp 
it would be termed a mosaic of the bluejoint 
reedgrass and beaked sedge herbaceous plant 
associations. 

No sensitive plant species were found. 

Copper Creek, Lower Drainage Wetlands: 

A large wetland, perhaps a fen in part, lies 
about Va mile southeast of the confluence of the 
Copper Creek and its tributary. North Fork 
Creek. This feature occupies what is probably 
a large kettle hole formed during the 
Pleistocene glaciation. This wetland is fed by 
subsurface seepage from the main stem of 
Copper Creek. The whole wetland was 
consumed with fire of varying intensities. The 
western-most portion of the wetland looks like 
an extensive carr (a type of fen with woody 
species prominent and, like all fens, having at 
least 30 cm of peat). The peat depth was not 
measured but in several places jumping on the 
surface created pressure waves that could be 
seen some distance away (typical of the 
floating mats of fens). This western portion 
had been burned very thoroughly with the shrub 
component currently sprouting prolifically but 
still between 1 and 3 dm tall. It appears that a 
mix of shrubs was present prior to the burn but 
now no one species could be recognized as 
dominant. Present are dwarf birch (Betula 
nana = B. glandulosa), diamondleaf willow. 
Tweedy 's willow, shrubby cinquef oil 
(Dasiphora floribunda = Potentilla fruticosa 
= Pentaphylloides floribunda), alderleaf 
buckthorn (Rhamnus alnifolia) and 
Engelmann spruce. Most stems of the spruce 
were killed and not sprouting. Beaked sedge is 
the dominant herb where these shrubs occur, 
with herb cover ranging widely from 10% - 



80%. Other conspicuous herbs are arrowleaf 
sweet coltsfoot (Petasites sagittata), largeleaf 
averts (Geum macrophyllum), small camas 
(Camassia quamash), alpine leafybract aster, 
purple marshlocks (Comarum palustre = 
Potentilla palustre), sticky cinquefoil 
(Potentilla glandulosa), wetland violet species 
{Viola spp.), alpine bentgrass {Agrsotis 
humilis) and Baltic rush {J uncus balticus). 
Several species of moss, all associated with 
rich carrs and fens, formed a nearly continuous 
ground cover. Moss species included (on 
hummocks) Tomenthypnum nitens. Sphagnum 
warnstorfii and (in swales, standing water) 
Scorpidium scorpioides, Limprichtia 
cossonii {Scorpidium cossonii), Limprichtia 
revolvens {Scorpidium revolvens), and 
Calliergon stramineum. 

Some areas, especially the eastern end of the 
wetland, never possessed a woody component 
[or this woody component occurred in 
dispersed, burned and formerly robust clumps 
of Geyer's {S. geryeri) and Drummond's 
willow {S. drummondii)] Beaked sedge is 
dominant, although in some places alpine 
bentgrass is a conspicuous component 
approaching co-dominance. The ground cover 
is a lawn of mosses with the following most 
prominent in declining order: Tomenthypnum 
nitens, Brachythecium salebrosum 
(= Brachythecium pseudocollinum), 
Limprichtia cossonii, and Sphagnum 
warnstorfii. Conspicuous patches, light green 
from a distance, are dominated by woolyfruit 
sedge {Carex lasiocarpa); this community has 
only a few vascular species including muhly 
{Muhlenbergia spp.), alpine bentgrass, beaked 
sedge, alpine leafybract aster, and common 
camas (C quamash). Also located in the 
eastern portion of the complex are extensive 
areas of fowl bluegrass {Poa palustris), both 
with and without beaked sedge; this 
composition along with the scattered patches of 
Canada thistle could be indicative of past 
disturbance. 

No sensitive vascular plant species were 
found here, but a more intensive inventory 



of the diverse bryophyte community could 
be rewarding. 

Keep Cool Lakes: These ponds have dried 
to "water weed" colonized mud flats due to the 
multi-year drought. Silts and clays have settled 
on a bottom of rounded, stream-worked rock. 
The mud flat is colonized by patches of 
buckbean {Menyanthes trifoliata) and various 
species of pondweed {Potamogeton spp.) and 
dock {Rumex spp.). Baltic rush {Juncus 
balticus) is also present and appears to be 
actively expanding from somewhat isolated 
patches. Near the inflow there is a moisture/ 
salinity gradient occupied by four relatively 
distinct communities. The driest sites are 
occupied by a nearly monospecific tufted 
hairgrass type that transitions into a moister 
tufted hairgrass with a dense sub-canopy of 
shortawn foxtail {Alopecurus aequalis). A 
pale false mannagrass {Torreyochloa pallida 
(Torr.) Church var. pauciflora (formerly 
Puccinellia pauciflora) type is next then the 
standing water condition (mostly 3-6 cm deep) 
supports common spikerush {Eleocharis 
palustris) in a virtual monoculture with the 
exception of scattered tussocks of tufted 
hairgrass and dock. 

The pale false mannagrass has a dense 
undergrowth of needle spikerush {Eleocharis 
acicularis); a community with this composition 
has not described for Montana (even as a 
dominance type) or other states. The substrate 
for this community appears to have a 
considerably higher clay content than the other 
communities and, if this species is similar to 
others in its genus like P. nuttalliana, then this 
community may reflect an alkaline substrate as 
well. On the margins of the upper pond 
(particularly in the area of inflow and nearby to 
the east and south) is an extensive zone of 
tufted hairgrass that has been invaded with 
timothy {Pleum pratense) and Kentucky 
bluegrass {Poa pratensis); this infestation is 
heaviest near an ATV trail (Figure 3) branching 
to the south around the pond. Canada thistle 
and common mullein {Yerbascum thapsus) 
have also established in this area with Canada 



thistle expanding into the muddy pond fringes. 
The ATV track is worn to the point that 
portions of this tufted hairgrass community 
have been denuded of vegetation. This track 
and areas immediately to either side are 
disturbed creating a prime weed establishment 
site, especially since the ATVs could also 
disperse weed seeds (which are abundant in 
the camping area). 




Figure 3. ATV track through Keep Cool Lake 
wetlands 

The ATV track goes on to connect the Upper 
with Lower Keep Cool Lake. Along this route, 
timothy has expanded extensively to dominate 
what could have been a species-rich blue 
wildrye (Elymus glaucus) dominated meadow. 
Blue wildrye is now is only scattered at the site. 
If true, this meadow, although probably not a 
jurisdictional wetland, could have been a unique 
meadow type (G2) known (as of 1998) from 
only California and Oregon (Anderson et al. 
1998) and not previously reported from 
Montana. The ATV trail continues to the 
perimeter of Lower Keep Cool Lake and, in at 
least two locations, there were massive 
disturbances where they had to be extricated 
from the mud. 

There is a small stand of willows at the head of 
the Lower Lake including Drummond's, 
Booth's, and Bebb's (S. bebbiana) willows; the 
vegetation association most similar is 
Drummond's willow / beaked sedge. Extending 
to both the north and south of the inlet and 
arcing around to the west is an extensive and 



typically species-poor beaked sedge association; 
common associates are swordleaf rush {Juncus 
ensifolius), wild bergamot (Monarda 
fistulosa) and, in standing water, pondweed. 
Along a more western portion of the northern 
shore a sort of reverse zonation was 
encountered where the wettest community, the 
beaked sedge association, was nearest the 
upland, giving way centripetally to a common 
spikerush - tufted hairgrass community, in turn 
grading to a nearly pure tufted hairgrass 
association and lastly to a saturated surface 
with water-filled mini-depressions and much 
exposed mud that has been uniquely, and 
virtually monospecifically, colonized by greater 
creeping spearwort {Ranunculus flammuld). 
Greater creeping spearwort is a common early 
colonizer of mudflats, especially those with 
brackish waters, but usually it occurs only as 
scattered plants, not as the almost continuous 
cover seen on the drawdown zone of Lower 
Keep Cool Lake. A visit at one point in time 
can not determine how ephemeral this condition 
might be, with continued drought and receding 
waters to expose mudflats this unique 
community may persist and expand vegetatively 
via stolons. 

No sensitive vascular species were 
documented at this local, but a unique 
community dominated by pale false 
mannagrass was associated with fine 
textured substrates. 

• Klondike Creek: A search was conducted 
both upslope and down (approximately 200 m in 
each direction) from the Beaver Creek Rd. 
crossing. This creek occurs in a V-notch 
drainage with steep (in excess of 40%) slopes 
(at least upslope of the road). The drainage 
configuration strongly constrained the type of 
wetlands represented. By far the most 
prevalent wetland was thinleaf alder (Alnus 
incana ssp. tenuifolia) dominated and confined 
to the immediate banks of the stream, only 
extending about 2 m away on mini-terraces in 
those uncommon places where the stream 
gradient was less. Undergrowth in these 
thinleaf alder thickets varied from a diversity of 



mesic forbs to virtually no undergrowth (two 
conditions recognized as separate associations). 
In some stretches, red-osier dogwood {Cornus 
sericea) was common, which is indicative of 
another type of thinleaf alder association. We 
did not detect abiotic variables that might have 
been responsible for the compositional 
differences. Most of the stream was 
entrenched enough that the bordering type was 
forested with the subalpine fir - Engelmann 
spruce / queencup beadlily plant association 
dominated by spruce, Douglas-fir (Pseudotsuga 
menziesii), and lodgepole pine. This association 
is not a wetland but is mesic to hygric in its 
moisture status and also lacks vegetation 
indicative of a wetland condition. Very small 
patches (fragments) of the subalpine fir - 
Engelmann spruce / claspleaf twistedstalk plant 
association also occur scattered immediately 
adjacent to the stream or in swales within the 
very narrow floodplain. 

Habitat adjacent to this stream is not 
conducive to supporting the sensitive plant 
species we were seeking. Cattle use is 
also considerable. 

Lincoln Gulch: This area encompasses the 
site of the first discovery (mid 1860's) of gold in 
this portion of the state; the activity, including 
dredging and pit excavations, continued until the 
turn of the century. In the ensuing lOO-i- years 
the area has largely reforested but the mark of 
mining is still omnipresent. The steam that 
courses through the gulch is ephemeral and, 
with the effects of past dredging, stream 
modification and downcutting, there is virtually 
no riparian or wetland communities. Most of 
the area is potentially dominated by the 
Engelmann spruce or Douglas-fir series; moister 
sites support the Engelmann spruce / queencup 
beadlily association, the Douglas-fir / common 
snowberry (Symphoricarpos albus) 
association is on dryer areas. The area 
probably does not support any jurisdictional 
wetlands but is clearly subirrigated since the 
swales support small patches of the Engelmann 
spruce - subalpine fir / red-osier dogwood 
association (where lodgepole pine, aspen 



[Populus tremuloides] and Douglas-fir are the 
usual serai dominants). Dogwood canopy cover 
ranges from about 10 to 40% and is heavily 
browsed to a somewhat uniform height of 1 to 
1.4 m. The undergrowth is dominated by a 
short to mid-shrub component dominated by 
common snowberry (to 80% canopy cover) and 
includes creeping barberry {Mahonia repens), 
common spiraea {Spiraea betulifolia), and 
russet buffaloberry (Shepherdia canadensis). 
The forb component of this association is 
weakly represented and includes sweetscented 
bedstraw (Galium triflorum), falsegold 
groundsel (Packera pseudaurea = Senecio 
pseudaureus), western meadowrue 
(Thalictrum occidentale), and starry false lily- 
of-the-valley (Maianthemum stellatum = 
Smilacina stellata), pink wintergreen (Pyrola 
asarifolia), and sweetcicely (Osmorhiza 
berteroi). Graminoids include blue wildrye, 
roughleaf ricegrass (Oryzopsis asperifolia), 
and false melic (Schizachne purpurascens). 
The excavated pit which ranges up to 3 m in 
depth contain red-osier dogwood since the 
slopes and bottoms are near the water-table. 
Dogwood shoots growing from the center of the 
deep pits are largely unbrowsed due to difficulty 
of animal access. 

Habitat adjacent to this ephemeral stream 
are not conducive to supporting the 
sensitive plant species we were seeking 
and true wetland communities are not 
present. 

Nolo Lakes: Located at about 6,400 and 6,500 
feet along the Meadow Creek Pack Trail these 
two water bodies have a considerably restricted 
wetland margin, approximately 1 to 5 m in 
width. The wettest community is a 
discontinuous fringe of water sedge that is 
primarily anchored in a thin unstable mud 
substrate; some of this community occupies the 
immediately surrounding stabilized, saturated 
and highly organic bank. The next drier 
community is a discontinuous zone typified by a 
robust sward of bluejoint reedgrass, in which 
arrowleaf ragwort and green false hellebore are 
important components. Occupying the most 



10 



extensive and slightly drier wetland habitat is a 
narrow forested zone dominated by well-spaced 
Engelmann spruce and very occasional 
subalpine fir with an undergrowth of scattered 
rusty menziesia, prickly current (Ribes 
lacustre), thinleaf or globe huckleberry 
(Vaccinium membranaceum), with grouse 
whortleberry in the mid-sized to dwarf shrub 
layer. Arrowleaf groundsel (Senecio 
triangularis), green false hellebore, claspleaf 
twis teds talk, and bluejoint reedgrass are the 
most abundant herbs, but their individual covers 
seldom exceeds 10%. The forested plant 
associations are a mosaic of Engelmann spruce 
/ bluejoint reedgrass on wetter sites and 
subalpine fir - Engelmann spruce / claspingleaf 
twistedstalk elsewhere. The latter association 
has a diversity of wet-site forbs but since rusty 
menziesia (M. ferruginea) has more than 5% 
cover this should be the rusty menziesia phase 
of this association (Cooper et al. 1985), a phase 
now elevated to plant association level 
(NatureServe 2005). The Nolo Lakes 
expression of this phase matches the modal 
condition, which is associated with frost pockets 
and soils with at least seasonally high water 
tables. 

No sensitive plant species were found and 
Nolo Lakes lack appropriate habitat for 
these species. 

Reservoir Lake: This water body appears to 
lack an outlet and has a water level determined 
by the prevailing climate. In this period of 
extended drought, the water level has been 
drawn down severely leaving a rocky 
unvegetated shoreline. At the high-watermark 
tufted hairgrass forms a nearly pure sward 
encircling the pond and extends over a rocky 
substrate to the surrounding forest comprised 
largely of subalpine fir / beargrass (Xerophyllum 
tenax) or subalpine fir / twinflower (Linnaea 
borealis) plant associations (Figure 4). Giant 
mountain aster and alpine leafybract aster, 
although very scattered, are the next most 
abundant herbs in the tufted hairgrass meadow 
type. The fewflower spikerush (Eleocharis 
quinqueflora = E. pauciflora) community 



colonizes the few, scattered and small mud 
flats. A common associate, although occurring 
with considerably less cover, is Poa secunda 
(the taxonomic entity once known as P. 
juncifolia, a robust, wetland-associated form 
of P. secunda). Much of the shoreline, particu- 
larly the drawdown zone, is being invaded by 
weedy species including oxeye daisy 
(Leucanthemum vulgare), white clover {Trifo- 
lium repens), timothy, and even spotted knap- 
weed (Centaurea biebersteinii). 

No sensitive plant species were found 
and Reservoir Lake lacks appropriate 
habitat for the species we are seeking. 




Figure 4. Drawdown zone at Reservoir Lake 

' Porcupine Basin: This is not actually a basin 
but is a reach of the North Fork of Arrastra 
Creek with a lesser gradient than the adjoining 
reaches in this vicinity. The area that might be 
considered a basin is predominantly forested 
with stands in the riparian portion dominated by 
Engelmann spruce and subalpine fir. 
Shrublands are confined to streamside stringers 
dominated by thinleaf alder and Sitka alder 
(Alnus viridis ssp. sinuata). The forested 
stands that would include true wetlands are of 
the subalpine fir - Engelmann spruce / rusty 
menziesia /claspingleaf twistedstalk plant 
association. Large (approaching a meter in 
diameter), widely spaced, often with missing 
mid to upper crown foliage, Engelmann spruce 
dominate the tree canopy with subalpine fir in 
the sub-canopy. The cover of rusty menziesia 
is generally in excess of 70%, mixed with much 



11 



lesser coverages of Sitka alder, thinleaf 
huckleberry (Vaccinium membranaceum), 
prickly current and rose spiraea. Beneath the 
dense shrub canopy forbs are not particularly 
abundant but are consistently present. Those 
indicative of high moisture status include 
claspleaf twistedstalk, green false hellebore 
(Veratrum viride), arrowleaf ragwort (Senecio 
triangularis), Lyall's angelica, softleaf sedge 
(Carex disperma); more generalist forbs 
included threeleaf foamflower (Tiarella 
trifoliata), queencup beadlily, Sitka valerian 
{Valeriana sitchensis), Hitchcock's smooth 
woodrush (Luzula glabrata var. hitchcockii), 
northwestern twayblade (Listera caurina), and 
northern licorice-root. This hygric to hydric 
association transitions upslope to a mesic forest 
typified by the Engelmann spruce - subalpine 
fir / rusty menziesia / queencup beadlily 
association. 

The most unique aspect of this area is the herb- 
dominated community (Figure 5) that occurs 
just upslope and to the west of the creek 
occupying deep and subirrigated (and/or 
seasonally saturated) silty soils derived from 
alluvium and coUuvium (based on vegetation 
composition alone this would be a wetland but 
hydrology is unknown and soils were neither 
mottled nor gleyed). This community would 
key to the arrowleaf ragwort herbaceous 
vegetation plant association but the Porcupine 
Basin representations are considerably more 
diverse than the modal conception of this 
association. Although arrowleaf ragwort is 
generally dominant (30-50% canopy cover), 
other forbs have up to 20% cover including 
subalpine fleabane (Erigeron peregrinus), 
Lyall's angelica, green false hellebore, western 
sweetroot (Osmorhiza occidentalis), 
sweetscented bedstraw, pioneer violet {Viola 
glabella), beargrass (Xerophyllum tenax), 
common cowparsnip (Heracleum maximum), 
broadleaf arnica, western meadowrue and 
Virginia strawberry (Frag aria virginiana). 
Blue wildrye was the dominant graminoid with 
up to 30% canopy cover; other graminoids 
included Pumpelly's brome (Bromus inermis 
ssp. pumpellianus) and mountain brome 



{Bromus marginatus). Despite abundant litter 
there was considerable bare ground due to the 
workings of pocket gophers (Thomomys 
talpoides). The most recently disturbed of 
these areas were dominated by fireweed 
(Chamerion angustifolium = Epilobium 
angustifolium), manyflower stickseed 
(Hackelia floribunda), western pearly 
everlasting (Anaphalis margaritacea), and a 
species of mustard. There was a shrub 
component but only on the periphery of the 
herbaceous community including thinleaf 
huckleberry, prickly current, and rosy spiraea. 
This meadow complex is probably excellent 
grizzly bear (Ursus arctos horribilis) habitat. 




Figure 5. Porcupine Basin wet meadow 






Porcupine Basin did not contain any of the 
sensitive plant species we are seeking, 
however, the putative occurrence (mature 
seeds required for positive identification) 
of northern licorice-root (Ligusticum 
verticillatum) is thought to be the 
easternmost documentation of this 
species, which is usually associated with 
the more moderate conditions of northern 
Idaho. 

Theodore Creek: This creek, at least the 
400m stretch upslope form Beaver Creek Rd. 
has a moderately steep gradient and is set in a 
V-notch (relatively narrow, < 20 m wide, flat 
bottom) in a forested environment. The only 
wetland vegetation is confined to streamside 
stringers of the thinleaf alder community type 



12 



(Hansen et al. 1995) and the subalpine fir - 
Engelmann spruce / claspleaf twistedstalk plant 
association. Both communities range from 
about 1 to 5 m in width and tend to border the 
subalpine fir / queencup beadlily plant 
association (Clintonia uniflora phase) on 
upslope or drier sites of the stream bench. 
Queencup beadlily, starry false lily-of-the-valley 
and twinflower dominate the undergrowth and 
various shrub species, including principally 
thinleaf huckleberry and thimbleberry (Rubus 
parviflorus), constitute less than 20% cover. 
For extensive stretches the forest, dominated by 
a variable mix of Engelmann spruce, lodgepole 
pine, Douglas-fir and subalpine fir, extends right 
to the creek bank with only the presence of the 
hydric indicators arrowleaf ragwort, claspleaf 
twistedstalk, green false hellebore and cow- 
parsnip serving to delimit the narrow wetland 
zone. Fragments of a relatively rare plant 
association, Engelmann spruce / softleaf sedge, 
occur in saturated to the surface small patches 
(mostly less than 16 m^) immediately adjacent to 
the creek. 



monitoring of recruitment through metamorphosis 
when larvae are about to metamorphose. Together 
these surveys would assess the effects of post fire 
habitat succession as well as anthropogenic effects 
of on and off road vehicle use and recreation, 
which might require management actions. 
Furthermore, regular monitoring of Western Toads 
would also allow all of the other lentic breeding 
amphibians and aquatic reptiles in the area to be 
monitored. 

Due to the paucity of records in the study area for 
Rocky Mountain Tailed Frogs, we also recommend 
systematic surveys of stream habitats in the area 
for this species. These could either be conducted 
as focal surveys targeting this species in order to 
thoroughly understand its distribution and ecological 
limits in the area, or may be combined with fishery 
surveys if costs of the first approach are 
prohibitive. In either case, it is important to submit 
all observations of this and other species to the 
Montana Natural Heritage Program so that this 
information can be placed in the statewide Point 
Observation Database. 



No sensitive plants were found, probably 
due to the lack of appropriate habitat but 
cattle grazing may also be important. 

Conclusions / 
Recommendations 

Herpetofauna 

Although Western Toads remain widespread in 
western Montana they now breed in a relatively 
small percentage of watersheds and lentic sites 
across the region. Because population strongholds 
(i.e., watersheds with a relatively high percent of 
sites used for breeding) are rare across western 
Montana, the relatively healthy populations in this 
region are noteworthy. Perhaps the highest priority 
for management of herpetofauna in the area would 
be to initiate a monitoring program for the species 
with two annual visual encounter surveys 
conducted at all sites where breeding has been 
detected. The first survey would target the period 
of amplexus in order to identify numbers of 
breeding adults and a second survey would allow 



Sensitive Plants & Communities 

About 30 of the 50 plant associations identified as 
having Global (G) or State (S) ranks of 3 or less (or 
undetermined (?)) which potentially occur within 
the study area were identified (Appendix B Table 
1). This represents considerable wetland and 
riparian diversity for this relatively arid region; 
additionally most of the wetlands are ecologically 
intact, although nonnative plants are established in 
some and are a considerable threat in all wetlands 
and riparian areas. 

One large wetland (Copper Creek, Lower 
Drainage site) contained an extensive carr, a type 
of fen, which is a very uncommon community type 
in Montana. This site also has an extensive 
bryophyte component and warrants further survey 
for this taxonomic group. The wetland would make 
a good candidate for studies of post-fire 
succession. 

At Porcupine Basin we putatively identified the 
easternmost documentation of Northern licorice- 
root, a species more typically found in mesic 



13 



northern Idaho. The lack of seeds for a positive 
identification suggests that another visit at the 
appropriate time would be worthwhile. 

Keep Cool Lakes has a community type that may 
have once been a species-rich blue wildrye 
meadow, a G2 rank community previously known 
only from California and Oregon. Nonnative 
timothy grass now dominates. While this site is still 
in relatively good ecological condition, it has an 
ATV trail through the wetland that typifies the 
range of damage that all accessible wetlands can 
experience. Nonnative plants were invading along 
the ATV track, large disturbances occurred where 
the vehicles were extricated from wet areas, and 
breeding sites for the Western Toad were only a 
few feet from the track. ATV use can quickly 
degrade otherwise intact wetlands if access is easy 
and not actively discouraged. 



Literature Cited 

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General Technical Report INT-236. Intermoun- 
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Grossman, D. H., D. Faber-Langendoen, A. S. 
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Heyer, W. R., M. A. Donnelly, R. W. McDiarmid, 
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14 



Maxell, B. A. 2000. Management of Montana's 
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Maxell, B. A., J. K. Werner, P. Hendricks, and D. 
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15 



Appendix A. Global/State Rank Definitions 



Heritage Program Ranks 

The international network of Natural Heritage Programs employs a standardized ranking system to denote 
global (range-wide) and state status. Species are assigned numeric ranks ranging from 1 to 5, reflecting 
the relative degree to which they are "at-risk". Rank definitions are given below. A number of factors are 
considered in assigning ranks — the number, size and distribution of known "occurrences" or populations, 
population trends (if known), habitat sensitivity, and threat. Factors in a species' life history that make it 
especially vulnerable are also considered (e.g., dependence on a specific pollinator). 

Global Rank Definitions (NatureServe 2003) 

G 1 Critically imperiled because of extreme rarity and/or other factors making it highly 

vulnerable to extinction 
G2 Imperiled because of rarity and/or other factors making it vulnerable to extinction 

G3 Vulnerable because of rarity or restricted range and/or other factors, even though it may 

be abundant at some of its locations 
G4 Apparently secure, though it may be quite rare in parts of its range, especially at the 

periphery 
G5 Demonstrably secure, though it may be quite rare in parts of its range, especially at the 

periphery 
Tl-5 Infraspecific Taxon (trinomial) — The status of infraspecific taxa (subspecies or 

varieties) are indicated by a "T-rank" following the species' global rank 

State Rank Definitions 

51 At high risk because of extremely limited and potentially declining numbers, 
extent and/or habitat, making it highly vulnerable to extirpation in the state 

52 At risk because of very limited and potentially declining numbers, extent and/or 
habitat, making it vulnerable to extirpation in the state 

53 Potentially at risk because of limited and potentially declining numbers, extent 
and/or habitat, even though it may be abundant in some areas 

54 Uncommon but not rare (although it may be rare in parts of its range), and usually 
widespread. Apparently not vulnerable in most of its range, but possibly cause for 
long-term concern 

55 Common, widespread, and abundant (although it may be rare in parts of its 
range). Not vulnerable in most of its range 

Combination Ranks 

G#G# or S#S# Range Rank — A numeric range rank (e.g., G2G3) used to indicate uncertainty about 
the exact status of a taxon 

Qualifiers 

NR Not ranked 

Q Questionable taxonomy that may reduce conservation priority — Distinctiveness of 

this entity as a taxon at the current level is questionable; resolution of this uncertainty may 
result in change from a species to a subspecies or hybrid, or inclusion of this taxon in 
another taxon, with the resulting taxon having a lower-priority (numerically higher) 
conservation status rank 



Appendix A - 1 



X Presumed Extinct — Species believed to be extinct throughout its range. Not located 

despite intensive searches of historical sites and other appropriate habitat, and virtually no 
likelihood that it will be rediscovered 

H Possibly Extinct — Species known from only historical occurrences, but may never-the- 

less still be extant; further searching needed 

U Unrankable — Species currently unrankable due to lack of information or due to substan- 

tially conflicting information about status or trends 

HYB Hybrid — Entity not ranked because it represents an interspecific hybrid and not a species 

? Inexact Numeric Rank — Denotes inexact numeric rank 

C Captive or Cultivated Only — Species at present is extant only in captivity or cultivation, 

or as a reintroduced population not yet established 

A Accidental — Species is accidental or casual in Montana, in other words, infrequent and 

outside usual range. Includes species (usually birds or butterflies) recorded once or only a 
few times at a location. A few of these species may have bred on the one or two occa- 
sions they were recorded 

Z Zero Occurrences — Species is present but lacking practical conservation concern in 

Montana because there are no definable occurrences, although the taxon is native and 
appears regularly in Montana 

P Potential — Potential that species occurs in Montana but no extant or historic occurrences 

are accepted 

R Reported — Species reported in Montana but without a basis for either accepting or 

rejecting the report, or the report not yet reviewed locally. Some of these are very recent 
discoveries for which the program has not yet received first-hand information; others are 
old, obscure reports 

SYN Synonym — Species reported as occurring in Montana, but the Montana Natural Heritage 

Program does not recognize the taxon; therefore the species is not assigned a rank 

* A rank has been assigned and is under review. Contact the Montana Natural Heritage 

Program for assigned rank 

B Breeding — Rank refers to the breeding population of the species in Montana 

N Nonbreeding — Rank refers to the non-breeding population of the species in Montana 



Appendix A - 2 



Appendix B. Tables 



Table 1. Inventory Targets for Plant Species of Concern and Highly Ranked Plant Communities'^ 



Scientific Name 


Common Name 


Global 
Rank 


State 
Rank 


Noted in 
survey 


Potentially Occurring Plant Species of Concern (alphabetically arranged by latin binomial) 


Carex chordorrihiza 


Creeping Sedge 






N 


Carex idahoa 


Idaho Sedge 






N 


Carex livida 


Pale Sedge 






N 


Carex rostrata 


Beaked Sedge 






N 


Cypripedium fasciculatum 


Clustered Lady's-slipper 






N 


Cypripedium parviflorum 


Small Yellow Lady's-slipper 






N 


Cypripedium passerinum 


Sparrow's-egg Lady's-slipper 






N 


Drosera anglica 


EngUsh Sundew 






N 


Drosera linearis 


Linear-leaved Sundew 






N 


Epipactis gigantea 


Giant Helleborine 






N 


Kalmia polifolia 


Pale Laurel 






N 


Lycopodium inundatum 


Northern Bog Clubmoss 






N 


Scirpus cespitosus 


Tufted Club-rush 






N 


Utricularia intermedia 


Flat-leaved Bladderwort 






N 


Potentially Occurring Wetland/Riparian Plant Communities with G or S Rank of 3 or less, or S = ? 


Abies lasiocarpa / Oplopanax horridus Forest 


Subalpine fir / Devil's-club Forest 






Y 


Abies lasiocarpa / Streptopus amplexifoliusFor&st 


Subalpine fir / Claspleaf twistedstalk Forest 






Y 


Abies lasiocarpa / Actaea rubra Forest 


Subalpine fir / Baneberry Forest 






Y 


Alnus incana - Betula occidentalis Shrubland 


Mountain alder - Water birch Shrubland 






N 


Alnus incana / Calamagrostis canadensis Shrubland 


Mountain alder / Bluejoint reedgrass Shrubland 






N 


Alnus incana / Carex spp. Shrubland 


Mountain alder / Sedge spp. Shrubland 






N 


Alnus incana / Cornus sericea Shrubland 


Mountain / Red-osier dogwood Shrubland 






Y 


Alnus incana / Equisetum arvense Shrubland 


Mountain alder / Field horsetail Shrubland 






N 


Alnus incana Mesic Forbs Shrubland 


Mountain alder / Mesic Forbs Shrubland 






Y 


Alnus incana Shrubland 


Mountain alder Shrubland 


G?Q 


S3 


Y 


Alnus viridis ssp. sinuata / Athyrium filix- femina Shrubland 


Sitka alder / Lady fern Shrubland 


G3G4 


S? 


N 


Alnus viridis ssp. sinuata Shrubland [Provisional] 


Sitka Alder Shrubland 


G?Q 


S2 


N 


Betula glandulosa / Carex cusickii Shrubland 


Bog birch / Cusick's sedge Shrubland 




S3 


N 


Betula occidentalis - Pentaphylloides floribunda Shrubland 


Water birch - Shrubby cinquefoil Shrubland 


G2QS? 


G2QS? 


N 


Betula occidentalis / Cornus sericea Shrubland 


Water birch / Red-osier dogwood Shrubland 


G3? 


S? 


N 


Betula occidentalis Shrubland 


Water birch Shrubland 


G3Q 


S3 


N 


Carex buxbaumii Herbaceous Vegetation 


Buxbaum's sedge Wet Meadow 


G3 


S3 


N 


Carex lanuginosa Herbaceous Vegetation 


Woolly sedge Herbaceous Vegetation 


G3 


S? 


N 


Carex limosa Herbaceous Vegetation 


Mud sedge Herbaceous Vegetation 


G2 


S2 


N 


Carex simulata Herbaceous Vegetation 


Analogue sedge Herbaceous Vegetation 


G4 


S3 


N 


Cornus sericea Shrubland [Provisional] 


Red osier dogwood Shrubland 


G4Q 


S3 


Y 


Cornus sericea / Galium triflorum Shrubland 


Red osier dogwood / 
Sweet-scented bedstraw Shrubland 


G3? 


S? 


N 


Crataegus douglasii Shrubland 


Black hawthorn Shrubland 


G2Q 


S2 


N 


Dasiphora fruticosa ssp. floribunda /Carex spp. Shrubland 


Shrubby cinquefoil / sedge spp. Shrubland 


G3? 


S3 


Y 


Dulichium arundinaceum Herbaceous Vegetation 


Threeway sedge Herbaceous Vegetation 


G3 


S2 


N 


Eleocharis quinqueflora Herbaceous Vegetation 


Few-flower spikerush Herbaceous Vegetation 


G4 


S3 


Y 


Eleocharis rostellata Herbaceous Vegetation 


Beaked spikerush Herbaceous Vegetation 




S1 


N 


Glyceria borealis Herbaceous Vegetation 


Northern mannagrass Wet Meadow 


G4 


S3 


N 



Appendix B - 1 



Table 1. Continued. 



Scientific Name 


Common Name 


Global 
Rank 


State 
Rank 


Noted in 
survey 


Phragmites australis Temperate Herbaceous Veg. 


Western reed Marsh 


G5 


S2 


N 


Picea engelmannii / Carex disperma Forest 


Engelmann spruce / Softleaf sedge Forest 


G2 


S? 


Y 


Picea engelmannii / Cornus sericea Woodland 


Engelmann spruce / Red-osier dogwood Wdlnd. 


G3 


S3 


N 


Picea engelmannii / Equisetum arvense Forest 


Engelmann spruce / Field horsetail Forest 


04 S2 


S2 


Y 


Picea engelmannii / Galium triflorum Forest 


Engelmann spruce / Sweet-scented bedstraw For. 


G4 


S? 


Y 


Populus balsamifera ssp. trichocarpa / Cornus sericea 
Forest 


Black Cottonwood / Red-osier dogwood Forest 


G3? 


S3? 


N 


Populus tremuloides / Calamagrostis canadensis Forest 


Quaking aspen / Bluejoint reedgrass Forest 


03 


S2 


N 


Populus tremuloides / Cornus sericea Forest 


Quaking aspen / Red-osier dogwood Forest 


G4 


S3 


N 


Populus tremuloides / Heracleum maximum Forest 


Quaking aspen / Common cowparsnip Forest 


G4Q 


S2? 


N 


Pseudotsuga menziesii/ Cornus sericea Woodland 


Douglas fir / Red-osier dogwood Woodland 


04 


S3 


N 


Salix Candida / Carex lasiocarpa Shrubland 


Hoary willow / Slender sedge Shrubland 




S? 


N 


Salix Candida / Carex utriculata Shrubland 


Hoary willow / Beaked sedge Shrubland 


G3 


S3 


N 


Salix drummondiana / Calamagrostis canadensis 
Shrubland 


Drummond's willow / 
Bluejoint reedgrass Shrubland 


G3 


S? 


Y 


Salix geyeriana / Carex aquatilis Shrubland 


Geyer's willow / Aquatic sedge Shrubland 


03 


S? 


Y 


Salix geyeriana / Deschampsia cespitosa Shrubland 


Geyer willow / Tufted hairgrass Shrubland 


G4 


S3 


Y 


Salix geyeriana /Mesic Graminoids Shrubland 


Geyer's willow / Mesic Graminoid Shrubland 


G3 


S? 


Y 


Salix planifolia / Calamagrostis canadensis Shrubland 


Planeleaf willow / Bluejoint reedgrass Shrubland 


04 


S? 


N 


Salix planifolia / Carex aquatilis Shrubland 


Planeleaf willow / Aquatic sedge Shrubland 


G5 


S3 


N 


Salix planifolia / Carex scopulorum Shrubland 


Planeleaf willow / 

Holm's Rocky Mountain Sedge Shrubland 


G3 


S? 


N 


Salix planifolia / Carex utriculata Shrubland 


Planeleaf willow / beaked sedge Shrubland 


G1 


S? 


N 


Salix wolf a / Deschampsia cespitosa Shrubland 


Wolf willow / tufted hairgrass Shrubland 


G3 


S3 


N 


Senecio triangularis Herbaceous Vegetation 


Arrowleaf ragwort Herbaceous Vegetation 


G5? 


S3? 


N 


Spiraea douglasii Shrubland 


Rose spiraea Shrubland 


G5 


S2 


Y 



* Communities without ranks are those recently described for Montana and not yet ranked. 



Appendix B - 2 



Table 2. Amphibian and reptile species detected during wetland site surveys. Heritage Program surveys were 
conducted in June and September 2004 and July 2005. Other observations at these sites in preceding years are 
included for reference. Site numbers correspond to those shown in figures. 



Site 
No. 


Site Name 


Township Range 

Section 

(elevation) 


Date 


Lead 

Surveyor & 

Duration 

(hr:min) 


Species 

a 


Comments 


1 


Upper Keep Cool Lake 


T15NR8WS34NWSE 

(4980 ft) 


6/1/2004 


Paul Hendricks 
3:10 


BUBO 
RALU 


3 ad., 6 egg strings 
5 ad., 17JUV., 1 tadpole 








7/29/2005 


Bryce Maxell 
0:57 


RALU 
THSI 


lad. 
lad. 


2 


Lower Keep Cool Lake 


T15NR8WS34SWSW 

(4940 ft) 


6/1/2004 


Paul Hendricks 
2:00 


RALU 
THSI 


6 ad. 
lad. 


3 


Indian Meadows pond 1 


T16NR8WS34NENW 
(6080 ft) 


6/2/2004 


Paul Hendricks 
1:40 


BUBO 
RALU 


1 ad., 800+ larvae 

2 juv. 








7/29/2005 


Bryce Maxell 
0:10 


AMMA 
RALU 


^100 larvae 
2 metamorphs 


4 


Indian Meadows pond 2 


T16NR8WS34NWNW 
(6065 ft) 


6/2/2004 


Paul Hendricks 
1:10 


BUBO 


1 ad. (calling) 








7/29/2005 


Bryce Maxell 
0:09 


BUBO 


200+ metamorphs 


5 


Indian Meadows pond 3 


T16NR8WS33NWNE 

(6040 ft) 


6/2/2004 


Paul Hendricks 
1:40 


BUBO 
RALU 


4 ad. (pair amplexed) 
1 subad. 








7/29/2005 


Bryce Maxell 
0:56 


AMMA 
RALU 


3 larvae 
2 juv. 


6 


Indian Meadows pond 4 


T16NR8WS33SWNE 

(6020 ft) 


6/2/2004 


Paul Hendricks 
0:50 


RALU 


3 juv., 10+ larvae 


7 


Indian Meadows pond 5 


T16NR8WS34SWNW 

(5950 ft) 


6/2/2004 


Paul Hendricks 
0:40 


RALU 


2 juv. 


8 


Upper Copper Lake 


T15NR9WS4SWSW 

(7220 ft) 


6/3/2004 


Paul Hendricks 
2:00 


AMMA 
RALU 


1 ad., 4 egg masses 
3 ad., 9 juv. 


9 


Upper Copper Lake pond 


T15NR9WS9NENW 

(7220 ft) 


6/3/2004 


Paul Hendricks 
0:40 


none 




10 


Lower Copper Lake 


T15NR9WS9SESE 

(6860 ft) 


6/3/2004 


Paul Hendricks 
0:30 


none 


large salmonids 


11 


Reservoir Lake 


T15NR10WS25SWNW 

(5470 ft) 


8/31/1995 


Jim Reichel 
Unknown duration 


none 










9/1/1996 


Bogaert, J. 
Unknown duration 


AMMA 


5 individuals 








5/23/2001 


Laura Burns 
Unknown duration 


AMMA 
BUBO 


200 individuals, 1 egg 
1 amplexed pair 








6/4/2004 


Paul Hendricks 
1:00 


BUBO 


19 ad., 2 egg strings 
(7 pairs amplexed) 








7/29/2005 


Bryce Maxell 
0:30 


AMMA 
BUBO 
RALU 


< 10,000 larvae 

< 100 larvae 
1 juv. 


12 


Unnamed wetland 


T15NR8WS3SWSE 

(5600 ft) 


9/8/2004 


Coburn Currier 
0:50 


RALU 


1 ad., 10 juv. 


13 


Unnamed wetland 


T15NR8WS3SESE 

(5630 ft) 


9/8/2004 


Coburn Currier 
0:20 


RALU 


3 ad., 29 juv. 


14 


Snowbank Lake 


T15NR8WS9NWNW 

(5300 ft) 


6/8/2001 


Mike Kaiser 
Unknown duration 


BUBO 


1 individual 








9/8/2004 


Coburn Currier 
0:50 


BUBO 


100s juv., 
1000s larvae 








7/29/2005 


Bryce Maxell 
0:56 


BUBO 
THEL 


< 10,000 larvae 
2 ad. 


15 


Copper Creek small pond 


T15NR8WS5NWNW 
(5400 ft) 


9/8/2004 


Coburn Currier 
0:30 


BUBO 


lad. 



^ AMMA (Ambystoma macrodactylum: long-toed salamander), ASMO (Ascaphus montanus: Rocky Mountain tailed frog), BUBO 
{Bufo boreas: western toad), RALU (Rana luteiventris: Columbia spotted frog), THEL (Thamnophis elegans: Terrestrial 
Gartersnake), THSI (Thamnophis sirtalis: common garter snake). 



Appendix B - 3 



Table 2. Continued. 



Site 
No. 


Site Name 


Township Range 

Section 

(elevation) 


Date 


Surveyor and 
Duration 
(hrrmin) 


Species^ 


Comments 


16 


Copper Creek big pond 


T15NR8WS5NWNW 
(5400 ft) 


5/24/1995 


Jim Reichel 
Unknown 
duration 


AMMA 
RALU 


7 egg masses 
lad. 








9/8/2004 


Coburn Currier 
1:10 


BUBO 
RALU 


1 ad., 1 juv. 
5 ad., 12 juv. 










Bryce Maxell 
0:46 


AMMA 
BUBO 
RALU 
THEL 


< 100 larvae 

< 100 larvae, 9 juv. 

< 100 larvae, 13 ad. 
2 ad. 


17 


Copper Creek wetlands 


T15NR8WS5NWNE 
(5350 ft) 


9/8/2004 


Coburn Currier 
2:10 


RALU 


1 ad., 6 juv., 
3 larvae 


18 


Copper Creek marsh 


T15NR8WS4NWSW 

(5340 ft) 


9/9/2004 


Coburn Currier 
0:30 


RALU 


2 ad. 


19 


Yukon Creek 


T15NR9WS29SESW 

(5000 ft) 


9/9/2004 


Coburn Currier 
2:40 


ASMO 
RALU 


1 ad., 29 larvae 
3 juv. 


20 


Klondike Creek 


T15NR9WS32NENE 
(4900 ft) 


9/9/2004 


Coburn Currier 
2:10 


ASMO 
BUBO 


21 larvae 
lad. 


21 


Blackfoot Oxbow 


T14NR10WS33SWSE 


8/25/1995 


Jim Reichel 
Unknown 
duration 


AMMA 
BUBO 
RALU 


1 larvae 

3 metamorphs 

10 ad., 43 juv 








7/6/2001 


Ryan Killackey 
1:00 


AMMA 
BUBO 
RALU 


< 100 larvae 

< 100 larvae 

< 100 larvae, 1 juv, 1 ad 








7/9/2002 


Franz Zikesch 
2:00 


AMMA 
BUBO 
RALU 


< 100 larvae 

< 10,000 larvae 
3 juv, 1 ad. 








7/25/2004 


Allison Greene 
Unknown 
duration 


BUBO 
RALU 


30 juv. 
lad. 








7/28/2005 


Bryce Maxell 
5:00 


AMMA 
BUBO 

RALU 
THEL 


< 1,000 larvae 
10,000+ larvae, 1,000+ 
metamorphs, 1 ad. 

< lOlarvae, 5 juv, 10 ad 
lad. 



"" AMMA (Ambystoma macrodactylum: long-toed salamander), ASMO (Ascaphus montanus: Rocky Mountain tailed frog), BUBO 
{Bufo boreas: western toad), RALU (Rana luteiventris: Columbia spotted frog), THEL (Thamnophis elegans: Terrestrial 
Gartersnake), THSI (Thamnophis sirtalis: common garter snake). 



Appendix B - 4 



Appendix C. Occurrence Maps of Herpetofauna 




Data Source 

• Heritage Program in 2004 and 2005 n 

* Amphibian Inventory Program W^^w^^^E 
+ Other Data in Heritage Database ^ 

Site Numbers Correspond to those in Table 2 



0.9 1.8 Miles 




M (} N T A N A 

Natural 
Heritage 
Program 



Figure 1. Long-toed Salamander (Ambystoma macro dactylum) 

Appendix C - 1 




Data Source 

• Heritage Program in 2004 and 2005 n 

• Amphibian Inventory Program yy 
+ Other Data in Heritage Database 

Site Numbers Correspond to those in Table 2 




0.9 1.8 Miles 
_J I 



/ M Natural 
U%>$^ Heritage 



Figure 2. Rocky Mountain Tailed Frog (Ascaphus montanus) 

Appendix C - 2 




N 



Data Source 

• Heritage Program in 2004 and 2005 

* Amphibian Inventory Program 
+ Other Data in Heritage Database 

Site Numbers Correspond to those in Table 2 



W^^^E 




0.9 1.8 Miles 
_J I 



\^ 



a Natural 

' Heritage 

Program 



Figure 3. Western Toad (Bufo boreas) 



Appendix C - 3 




Data Source 

• Heritage Program in 2004 and 2005 n 

• Amphibian Inventory Program yy 
+ Other Data in Heritage Database 

Site Numbers Correspond to those in Table 2 




0.9 1.8 Miles 
_J I 




M {} N T A N A 

Natural 
Heritage 
Program 



Figure 4. Columbia Spotted Frog (Rana luteiventris) 

Appendix C - 4 




Data Source 

• Heritage Program in 2004 and 2005 

• Amphibian Inventory Program 

+ Other Data in Heritage Database 



N 
S 



0.9 1.8IVIiles 
_J I 




M (} N T A N A 

Natural 
Heritage 
Program 



Site Numbers Correspond to those in Table 2 



Figure 5. Terrestrial Gartersnake (Thamnophis elegans) 

Appendix C - 5 




Data Source 

• Heritage Program in 2004 and 2005 

* Amphibian Inventory Program 
+ Other Data in Heritage Database 

Site Numbers Correspond to those in Table 2 



N 



S 



0.9 1.8 Miles 
I \ I 



/^ j^^^ M {} N T A N A 

/ M Natural 
\a^3 Heritage 



Figure 6. Common Gartersnake (Thamnophis sirtalis) 

Appendix C - 6